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Gunung Berlin

Berlin

Tipe
Gunung api perisai
Ketinggian
3478 m
Letusan terakhir
-8350
Gunung Berlin
Public domain · Wikimedia Commons
Tipe
Gunung api perisai
Negara
Antarktika
Wilayah
Antarktika & Scotia / Western Antarctica Volcanic Province
Ketinggian
3478 m
Koordinat
-76.050, -136.000
Letusan terakhir
-8350
Kondisi tektonik
Intralempeng / Kerak benua (> 25 km)
Bentuk lahan
Perisai
Batuan utama
Trakit / Trakidasit
Ringkasan geologi

Mount Berlin consists of two coalescing shield volcanoes, Berlin Crater and Merrem Peak, each with a 2-km-wide summit caldera. Mount Berlin is located in the Flood Range of Marie Byrd Land, near the eastern coast of the Ross Sea. The two calderas are oriented along an east-west line, characteristic of Flood Range volcanoes. The westernmost and highest volcano, Berlin Crater, reaches 3478 m and is located 3.5 km ESE of Merrem Peak caldera. Berlin Crater displays active fumaroles along its western and northern caldera rims, producing the characteristic Antarctic fumarolic ice towers. The youngest dated tephra of a series of tephra layers in glacial ice at Mount Moulton that was attributed to Mount Berlin had an age of about 14.5 +/- 3.8 thousand years (ka), and a younger undated tephra layer was present. A lava flow at the base of an ice cave below a fumarolic ice tower was dated at about 10.3 +/- 2.7 ka.

Ringkasan Wikipedia

Ringkasan Inggris

Mount Berlin is a glacier-covered volcano in Marie Byrd Land, Antarctica, 100 kilometres (62 mi) from the Amundsen Sea. It is a roughly 20-kilometre-wide (12 mi) mountain with parasitic vents that consists of two coalesced volcanoes: Berlin proper with the 2-kilometre-wide (1.2 mi) Berlin Crater and Merrem Peak with a 2.5-by-1-kilometre-wide crater, 3.5 kilometres (2.2 mi) away from Berlin. The summit of the volcano is 3,478 metres (11,411 ft) above sea level. It has a volume of 200 cubic kilometres (48 mi3) and rises from the West Antarctic Ice Sheet. It is part of the Marie Byrd Land Volcanic Province. Trachyte is the dominant volcanic rock and occurs in the form of lava flows and pyroclastic rocks.

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8350 SM~8350 SM · 1 letusan · VEI maks. 08350 SM8350 SM8349 SM8349 SM8349 SM

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  1. 8350 SM (±5300 tahun)VEI 0Perkiraan geologi
    8350 SM – akhir tidak diketahui

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